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DOI | 10.1029/2018GL081364 |
Rupture Model of the M5.8 Pawnee, Oklahoma, Earthquake From Regional and Teleseismic Waveforms | |
Moschetti, M. P.1; Hartzell, S. H.1; Herrmann, R. B.2 | |
2019-03-16 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2019 |
卷号 | 46期号:5页码:2494-2502 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | The 2016 M5.8 Pawnee, Oklahoma, earthquake is the largest earthquake to have been induced by wastewater disposal. We infer the coseismic slip history from analysis of apparent source time functions and inversion of regional and teleseismic P waveforms, using aftershocks as empirical Green's functions. The earthquake nucleated on the shallow part of the fault, initially rupturing toward the surface, followed shortly thereafter by slip deeper on the fault. Deeper slip occurred below the aftershocks and at greater depths than most induced seismicity in the region, suggesting that small- to moderate-sized earthquakes may not occur on deeper parts of faults in Oklahoma because they are further from failure than shallower fault sections. Comparisons with models of pore pressure perturbations further suggest that the earthquake may have initiated within a region of higher pore pressure perturbation but was not confined to this zone. These observations inform source physics and understanding of maximum magnitudes. Plain Language Summary We analyzed seismic recordings from the 2016 M5.8 Pawnee, Oklahoma, earthquake to examine how the earthquake ruptured in time and how slip occurred on different parts of the fault. Our results show that the earthquake started on the shallow part of the fault, followed by slip toward the surface and slip occurring on the deeper part of the fault. By comparing our results with a previous study of changes in pore fluid pressures caused by injection, we find that the earthquake may have started where pore pressures were affected, but that the earthquake process continued outside of this region. That earthquake rupture can extend outside of the areas directly affected by injection processes is important for understanding maximum magnitudes from induced earthquakes. |
英文关键词 | induced earthquakes finite-fault inversion Oklahoma apparent source time functions |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000462612900019 |
WOS关键词 | W 5.8 PAWNEE ; SEISMIC-HAZARD FORECAST ; EASTERN UNITED-STATES ; SURFACE DEFORMATION ; FLUID INJECTION ; INVERSION ; AFTERSHOCKS ; FAIRVIEW ; INCREASE ; SLIP |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/181609 |
专题 | 气候变化 |
作者单位 | 1.US Geol Survey, Box 25046, Denver, CO 80225 USA; 2.St Louis Univ, Dept Earth & Atmospher Sci, St Louis, MO 63103 USA |
推荐引用方式 GB/T 7714 | Moschetti, M. P.,Hartzell, S. H.,Herrmann, R. B.. Rupture Model of the M5.8 Pawnee, Oklahoma, Earthquake From Regional and Teleseismic Waveforms[J]. GEOPHYSICAL RESEARCH LETTERS,2019,46(5):2494-2502. |
APA | Moschetti, M. P.,Hartzell, S. H.,&Herrmann, R. B..(2019).Rupture Model of the M5.8 Pawnee, Oklahoma, Earthquake From Regional and Teleseismic Waveforms.GEOPHYSICAL RESEARCH LETTERS,46(5),2494-2502. |
MLA | Moschetti, M. P.,et al."Rupture Model of the M5.8 Pawnee, Oklahoma, Earthquake From Regional and Teleseismic Waveforms".GEOPHYSICAL RESEARCH LETTERS 46.5(2019):2494-2502. |
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